Cite
Stability of a hydrous δ-phase, AlOOH–MgSiO2(OH)2, and a mechanism for water transport into the base of lower mantle
MLA
Masahiko Nishijima, et al. “Stability of a Hydrous δ-Phase, AlOOH–MgSiO2(OH)2, and a Mechanism for Water Transport into the Base of Lower Mantle.” Earth and Planetary Science Letters, vol. 401, Sept. 2014, pp. 12–17. EBSCOhost, widgets.ebscohost.com/prod/customlink/proxify/proxify.php?count=1&encode=0&proxy=&find_1=&replace_1=&target=https://search.ebscohost.com/login.aspx?direct=true&site=eds-live&scope=site&db=edsair&AN=edsair.doi...........4b913b71f49bddaa2a3bed4396d03c57&authtype=sso&custid=ns315887.
APA
Masahiko Nishijima, Takeshi Sakai, Naohisa Hirao, Masaaki Miyahara, Itaru Ohira, Yasuo Ohishi, & Eiji Ohtani. (2014). Stability of a hydrous δ-phase, AlOOH–MgSiO2(OH)2, and a mechanism for water transport into the base of lower mantle. Earth and Planetary Science Letters, 401, 12–17.
Chicago
Masahiko Nishijima, Takeshi Sakai, Naohisa Hirao, Masaaki Miyahara, Itaru Ohira, Yasuo Ohishi, and Eiji Ohtani. 2014. “Stability of a Hydrous δ-Phase, AlOOH–MgSiO2(OH)2, and a Mechanism for Water Transport into the Base of Lower Mantle.” Earth and Planetary Science Letters 401 (September): 12–17. http://widgets.ebscohost.com/prod/customlink/proxify/proxify.php?count=1&encode=0&proxy=&find_1=&replace_1=&target=https://search.ebscohost.com/login.aspx?direct=true&site=eds-live&scope=site&db=edsair&AN=edsair.doi...........4b913b71f49bddaa2a3bed4396d03c57&authtype=sso&custid=ns315887.